Characterising groundwater–surface water interactions in idealised ephemeral stream systems

Transmission losses from the beds of ephemeral streams are thought to be a widespread mechanism of groundwater recharge in arid and semi‐arid regions and support a range of dryland hydro‐ecology. Dryland areas cover ~40% of the Earth's land surface and groundwater resources are often the main s...

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Veröffentlicht in:	Hydrological processes 2020-08, Vol.34 (18), p.3792-3806
Hauptverfasser:	Quichimbo, Edisson A., Singer, Michael B., Cuthbert, Mark O.
Format:	Artikel
Sprache:	eng
Schlagworte:	Aeration zone Aquifers Arid lands Arid regions Arid zones Deep water Depth Depth indicators dryland hydrology Earth surface Ecology Ephemeral streams Feedback Fluxes Freshwater Groundwater Groundwater recharge Groundwater resources Groundwater table Hydraulic properties Hydraulics Infiltration Inland water environment Mathematical models Numerical models Permeability Resource management Rivers Sediments Stream discharge Stream flow Streambeds Streams stream–aquifer interactions Surface water Surface-groundwater relations Transmission loss Water depth Water exchange Water management Water resources Water resources management Water table
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